•
H. kjerulfi occurs in the Lower Cambrian of Norway (near Tomten, Sparagmite Formation,
Mjøsen, Atdabanian, 60.9° N, 10.7° E), and Poland (Ocieseki Sandstone Formation,
Holy Cross Mountains, Atdabanian, 51.0° N, 20.0° E). •
H. grandis occurs in the Lower Cambrian of Norway (near Tomten, Sparagmite Formation, Mjøsen, Atdabanian, 60.9° N, 10.7° E). •
H. glabra and
H. orienta are found in the Lower Cambrian of Poland (Ocieseki Sandstone Formation, Holy Cross Mountains, Atdabanian). •
H. lapponica was found in the Lower Cambrian of Sweden (Grammajukku Formation,
Holmia kjerulfi-zone, on the NE shore of Lake Långvattnet near Långsjöby, 10 km W of the village of
Storuman, county of Västerbotten, southern Swedish Lapland). •
H. palpebra was collected from the Lower Cambrian of Sweden (Upper part of the Grammajukku Formation, in the
Holmia kjerulfi-zone, E bank of the Torbacken rivulet, about 600 m South-Southwest of , the Laisvall area, central Swedish Lapland). • Unidentified specimen probably belonging to
Holmia are also known from the Lower Cambrian of Morocco (Issafen Formation,
Antatlasia gutta-pluviae/
Sectigena-zone, Atdabanian), and Sweden (shore 600 m North of , Gislöv Formation, Atdabanian (55.5° N, 14.3° E).